Observational data in July 2003. (A) Hourly air temperature and daily precipitation at Glomfjord 30 m a.s.l. and 18 km from Engabreen; (B) discharge at Fonndal station and calculated subglacial discharge; (C) load cell pressure records for LC6 and LC4; (D) and for LC97_1 and LC97_2. The shaded period is shown in Figure 4.
This figure is a high-resolution before-proof-read version of figure 3 published in Lefeuvre
P-M, Zwinger T, Jackson M, Gagliardini O, Lappegard G and Hagen
JO (2018) Stress Redistribution Explains Anti-correlated Subglacial
Pressure Variations. Front. Earth Sci. 5:110. https://doi.org/10.3389/feart.2017.00110
Cite this paper if you use the figure
Funding
Nordic Centre of Excellence SVALI, “Stability and Variations of Arctic Land Ice”, funded by the Nordic Top-level Research Initiative (TRI); Nordic Centre of Excellence eSTICC, “eScience tools for investigating Climate Change in Northern High Latitudes”